|
Like
other toxic metals, such as chromium and uranium, zinc undergoes many
chemical transformations during its journey from the source to the
final resting place. The Imperial Smelting Process used for many decades
in Europe produced considerable amounts of dust and fumes rich in
zinc and lead. When the zinc reached the soil, it was deposited in
the form of a number of "primary" zinc-containing minerals. Weathering
of these minerals resulted in the trapping of zinc in "secondary"
minerals, predominantly clay minerals but to a lesser extent iron
oxyhydroxides and manganese oxides that immobilize the zinc, rendering
it less harmful.
In recent years, x-ray
diffraction and EXAFS of powder samples have been replacing older
chemical-extraction techniques for speciation of contaminants in
the environment. Making EXAFS measurements for a large number of
compounds in well-prepared forms results in a library of standards
that can be used when a sample contains multiple chemical compounds
containing the same element. Mathematically fitting a combination
of the EXAFS spectra from standards with the measured spectrum in
principle identifies and gives the concentration of each compound
in the sample. However, the method does not work well when too many
standards are required, so it is necessary to have some idea of
what is present, a difficult task when some compounds exist in small
concentrations against a larger background of other compounds.
|
Molecular Environmental Science
|
The French team attacked
this problem for its soil samples by exploiting the newer third-generation
synchrotron-radiation sources. Powder EXAFS hinted that zinc-containing
clay minerals were the predominant species. Because of the layered
structure of clays, EXAFS spectra with linearly polarized light
has a distinctive angular dependence as an oriented sample is rotated
in the beam, and this is what the team observed at the ESRF. A detailed
analysis of the spectra revealed the local structure around the
zinc in the clay.
| Micro-EXAFS
of zinc in a manganese-rich area (red) of a soil sample identifies
the presence of zinc-sorbed birnessite (blue), a layered manganese
compound with zinc above and below vacant sites, as shown in the model. |
The two next most important
zinc species (i.e., the iron oxyhydroxides and manganese oxides) were identified
at the ALS. First, with µ-XRF, the team located regions containing manganese,
iron, and zinc in these inhomogeneous samples. In particular, they found
iron-rich grains that typically were 10 to 20 µm in size and manganese-rich
spherules much larger at 300 µm. Application of µ-EXAFS within these regions
then revealed the identity and structure of the zinc species. For example,
the zinc-containing manganese compound was birnessite, a layered compound
in which the zinc was adsorbed in the interlayer space above and below vacant
sites with either four- or six-fold coordination. Model compounds derived
from polarized and µ-EXAFS data were then used to obtain good fits of powder-EXAFS
data for all the soil samples studied.

Model
compounds derived from polarized-EXAFS data at the ESRF and µ-EXAFS
data at the ALS provide a good fit with powder-EXAFS spectra from
a soil sample.
Research conducted by A. Manceau, B. Lanson, M. L. Schlegel, J.-C. Hargé,
M. Musso, and J.-L. Hazemann (University J. Fourier and CNRS, France);
D. Chateigner (University of Maine-Le Mans, France) and G. M. Lamble (ALS).
Funding: DGAD/SRAE Division of the French Ministry of Environment (MATE)
and U. S. Department of Energy, Office of Basic Energy Sciences.
Publication about this experiment: A. Manceau et al., "Quantitative
Zn speciation in smelter-contaminated soils by EXAFS spectroscopy," Am.
J. Sci. 300, 289 (2000).
ALSNews Vol.
146, February 16, 2000 |